Monitoring one of the tipping points of the AMOC
Abstract The deep limb of the AMOC is fed by two main sources: a western source generated by deep convection in the Labrador/Irminger seas, and an eastern source originating in overflow of dense water from the Nordic Seas across the Greenland-Scotland Ridge, which is enhanced by water entrained afte...
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ftzenodo:oai:zenodo.org:1188871 2024-09-15T18:09:22+00:00 Monitoring one of the tipping points of the AMOC Larsen, Karin Margretha H. Hansen, Bogi Østerhus, Svein 2018-03-05 https://doi.org/10.5281/zenodo.1188871 eng eng Zenodo https://zenodo.org/communities/eu https://zenodo.org/communities/blue-actionh2020 https://doi.org/10.5281/zenodo.1188870 https://doi.org/10.5281/zenodo.1188871 oai:zenodo.org:1188871 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode OSM 2018, 2018 Ocean Sciences Meeting, Portland, Oregon, US, 11.-16. February 2018 AMOC Tipping point Monitoring Greenland-Scotland Ridge info:eu-repo/semantics/conferencePoster 2018 ftzenodo https://doi.org/10.5281/zenodo.118887110.5281/zenodo.1188870 2024-07-25T19:29:08Z Abstract The deep limb of the AMOC is fed by two main sources: a western source generated by deep convection in the Labrador/Irminger seas, and an eastern source originating in overflow of dense water from the Nordic Seas across the Greenland-Scotland Ridge, which is enhanced by water entrained after passing the ridge. These two sources behave very differently. The intensity of the western source varies dramatically from one year to another. Two decades of monitoring, in contrast, reveal that the overflow is remarkably stable. In the simple thermohaline paradigm, the generation and maintenance of overflow is linked to the properties of the compensating inflow of Atlantic water to the Nordic Seas, especially its salinity and hence its density after cooling. Watching how far this part of the AMOC is from a potential tipping point therefore involves observing the transport of mass and properties of the overflow and the inflow. Here, we focus on the densest of the overflow branches, the Faroe Bank Channel (FBC) overflow and the strongest of the Atlantic inflow branches, the Faroe Current (FC). During the last two decades, the volume transports of both these flows have remained stable with perhaps a weak increase, but the properties have changed. After the mid-1990s, both the temperature and the salinity of the FC increased. Similar trends have been observed for the FBC-overflow, although somewhat delayed and much reduced. Thus, the FBC-overflow has remained stable in density as well as volume transport. Since 2016, however, there has been a dramatic reduction in the salinity of the FC and hence the transport of salt into the generation area of the overflow water. Future monitoring of the Greenland-Scotland Ridge exchanges and its properties, thus, has a high priority, and emphasizes the need to continuously develop the monitoring systems and integrate them with remote sensing and new technology. Conference Object Greenland Greenland-Scotland Ridge Nordic Seas Zenodo |
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Open Polar |
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Zenodo |
op_collection_id |
ftzenodo |
language |
English |
topic |
AMOC Tipping point Monitoring Greenland-Scotland Ridge |
spellingShingle |
AMOC Tipping point Monitoring Greenland-Scotland Ridge Larsen, Karin Margretha H. Hansen, Bogi Østerhus, Svein Monitoring one of the tipping points of the AMOC |
topic_facet |
AMOC Tipping point Monitoring Greenland-Scotland Ridge |
description |
Abstract The deep limb of the AMOC is fed by two main sources: a western source generated by deep convection in the Labrador/Irminger seas, and an eastern source originating in overflow of dense water from the Nordic Seas across the Greenland-Scotland Ridge, which is enhanced by water entrained after passing the ridge. These two sources behave very differently. The intensity of the western source varies dramatically from one year to another. Two decades of monitoring, in contrast, reveal that the overflow is remarkably stable. In the simple thermohaline paradigm, the generation and maintenance of overflow is linked to the properties of the compensating inflow of Atlantic water to the Nordic Seas, especially its salinity and hence its density after cooling. Watching how far this part of the AMOC is from a potential tipping point therefore involves observing the transport of mass and properties of the overflow and the inflow. Here, we focus on the densest of the overflow branches, the Faroe Bank Channel (FBC) overflow and the strongest of the Atlantic inflow branches, the Faroe Current (FC). During the last two decades, the volume transports of both these flows have remained stable with perhaps a weak increase, but the properties have changed. After the mid-1990s, both the temperature and the salinity of the FC increased. Similar trends have been observed for the FBC-overflow, although somewhat delayed and much reduced. Thus, the FBC-overflow has remained stable in density as well as volume transport. Since 2016, however, there has been a dramatic reduction in the salinity of the FC and hence the transport of salt into the generation area of the overflow water. Future monitoring of the Greenland-Scotland Ridge exchanges and its properties, thus, has a high priority, and emphasizes the need to continuously develop the monitoring systems and integrate them with remote sensing and new technology. |
format |
Conference Object |
author |
Larsen, Karin Margretha H. Hansen, Bogi Østerhus, Svein |
author_facet |
Larsen, Karin Margretha H. Hansen, Bogi Østerhus, Svein |
author_sort |
Larsen, Karin Margretha H. |
title |
Monitoring one of the tipping points of the AMOC |
title_short |
Monitoring one of the tipping points of the AMOC |
title_full |
Monitoring one of the tipping points of the AMOC |
title_fullStr |
Monitoring one of the tipping points of the AMOC |
title_full_unstemmed |
Monitoring one of the tipping points of the AMOC |
title_sort |
monitoring one of the tipping points of the amoc |
publisher |
Zenodo |
publishDate |
2018 |
url |
https://doi.org/10.5281/zenodo.1188871 |
genre |
Greenland Greenland-Scotland Ridge Nordic Seas |
genre_facet |
Greenland Greenland-Scotland Ridge Nordic Seas |
op_source |
OSM 2018, 2018 Ocean Sciences Meeting, Portland, Oregon, US, 11.-16. February 2018 |
op_relation |
https://zenodo.org/communities/eu https://zenodo.org/communities/blue-actionh2020 https://doi.org/10.5281/zenodo.1188870 https://doi.org/10.5281/zenodo.1188871 oai:zenodo.org:1188871 |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode |
op_doi |
https://doi.org/10.5281/zenodo.118887110.5281/zenodo.1188870 |
_version_ |
1810446891763105792 |